The U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers, used an existing, three-dimensional, numerical ground-water flow model (referred to as the calibrated model) to assess the effects of water-level changes in the Mississippi River and Pokegama Reservoir on ground-water levels in adjacent glaciofluvial aquifers in the Grand Rapids area of north-central Minnesota. Pokegama Reservoir consists of Pokegama Lake, Little Jay Gould Lake, Jay Gould Lake, Cut-off Lake, and Blackwater Lake. Water levels in the Pokegama Reservoir are regulated at Pokegama Dam on the Mississippi River west of Grand Rapids. A steady-state model was used, and simulations represent “worse-case” scenarios for the effects of lowering or raising the river and lake water levels. The simulated ground-water levels represent levels that would result if the river and lake stages permanently declined or rose by the specified amounts. Eight hypothetical scenarios were simulated by varying water levels in the Mississippi River and Pokegama Reservoir from values used in the calibrated model. In the simulations, water levels for the Mississippi River, riverine wetlands of the Mississippi River, and lakes of the Pokegama Reservoir were raised and lowered uniformly by 0.50, 1.00, 2.00, and 3.00 feet from calibrated water levels.
\nThe extent of aquifer water-level changes resulting from these river, wetland, and lake water-level changes varied because of the complex hydrogeology of the study area. A 1.00-foot decline in reservoir/river water levels caused a maximum simulated ground-water-level decline in the middle aquifer near Jay Gould and Little Jay Gould Lakes of 1.09 feet and a maximum simulated ground-water-level decline of 1.00 foot in the lower aquifer near Cut-off and Blackwater Lakes. The amount and extent of ground-water-level changes in the middle and lower aquifers can be explained by the thickness, extent, and connectivity of the aquifers. Surface-water/ground-water interactions near wetlands and lakes with water levels unchanged from the calibrated model resulted in small water-table altitude differences among the simulations. Results of the ground-water modeling indicate that lowering of the reservoir and river water levels by 1.00 foot likely will not substantially affect water levels in the middle and lower aquifers.
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Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1425","title":"Lithology, hydraulic properties, and water quality of the Sandstone Aquifer in the northwestern part of the Bad River Indian Reservation, Wisconsin, 1998-1999","docAbstract":"The Precambrian sandstone aquifer in the northwestern part of the Bad River Band of Lake Superior Tribe of Chippewa Indians Reservation, Ashland County, Wisconsin, provides much of the drinking water to area residents. A study was undertaken in cooperation with the Bad River Tribe to provide specific information about the lithology, hydraulic properties, and water quality of the sandstone aquifer. During 1998 and 1999, the U.S. Geological Survey installed three monitoring wells, collected and analyzed lithologic and water samples, and conducted geophysical logging and aquifer tests to characterize the sandstone aquifer. The two monitoring wells in the southeastern part of the study area, the Diaperville Monitoring Well #1 (Diaperville MW #1) and the Tolman Monitoring Well #1 (Tolman MW #1) , are believed to have encountered older Middle Proterozoic Oronto Group sandstones. The sandstone encountered in the Ackley Monitoring Well #1 (Ackley MW #1) is believed to be Chequamegon Sandstone of the Late Proterozoic Bayfield Group. This interpretation is based on previous studies, as well as thin- section analysis of sandstone core recovered from the Ackley Monitoring Well #1. Results of aquifer tests conducted in the Diaperville Monitoring Well #1 and the Tolman Monitoring Well #1 provide ranges for hydraulic param - eter values in the sandstone aquifer: transmissivity ranges from 83 to 509 square feet per day; hydraulic conductivity ranges from 1.6 to 4.5 feet per day; storativity ranges from 0.00019 to 0.00046; and specific capacity ranges from 0.22 to 0.67 gallons per minute per foot. Though high- and low-angle fractures are present in Ackley Monitoring Well #1 core, the hydraulic properties of the bedrock appear to be due largely to the matrix porosity measured in thin section (16–21 percent) and permeability of the sandstone. The aquifer test for the Diaperville Monitoring Well #1 resulted in observed drawdown in nearby glacial wells, evidence of a hydraulic connection between the sandstone aquifer and the glacial deposits. Major ion analyses indicate that the water sampled from the sandstone aquifer at the Ackley site is of the calcium-magnesium-sodium- bicarbonate type. Based on a single sampling set, volatile organic constituents were not detected in water samples from the Diaperville Monitoring Well #1 or the Ackley Monitoring Well #1.
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Charles P. cdunning@usgs.gov","contributorId":892,"corporation":false,"usgs":true,"family":"Dunning","given":"Charles P.","email":"cdunning@usgs.gov","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":283534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71038,"text":"sir20045287 - 2005 - Rainfall-Runoff and Water-Balance Models for Management of the Fena Valley Reservoir, Guam","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"sir20045287","displayToPublicDate":"2005-08-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5287","title":"Rainfall-Runoff and Water-Balance Models for Management of the Fena Valley Reservoir, Guam","docAbstract":"The U.S. Geological Survey's Precipitation-Runoff Modeling System (PRMS) and a generalized water-balance model were calibrated and verified for use in estimating future availability of water in the Fena Valley Reservoir in response to various combinations of water withdrawal rates and rainfall conditions. Application of PRMS provides a physically based method for estimating runoff from the Fena Valley Watershed during the annual dry season, which extends from January through May. Runoff estimates from the PRMS are used as input to the water-balance model to estimate change in water levels and storage in the reservoir.\r\n\r\nA previously published model was calibrated for the Maulap and Imong River watersheds using rainfall data collected outside of the watershed. That model was applied to the Almagosa River watershed by transferring calibrated parameters and coefficients because information on daily diversions at the Almagosa Springs upstream of the gaging station was not available at the time. Runoff from the ungaged land area was not modeled. For this study, the availability of Almagosa Springs diversion data allowed the calibration of PRMS for the Almagosa River watershed. Rainfall data collected at the Almagosa rain gage since 1992 also provided better estimates of rainfall distribution in the watershed. In addition, the discontinuation of pan-evaporation data collection in 1998 required a change in the evapotranspiration estimation method used in the PRMS model. These reasons prompted the update of the PRMS for the Fena Valley Watershed.\r\n\r\nSimulated runoff volume from the PRMS compared reasonably with measured values for gaging stations on Maulap, Almagosa, and Imong Rivers, tributaries to the Fena Valley Reservoir. On the basis of monthly runoff simulation for the dry seasons included in the entire simulation period (1992-2001), the total volume of runoff can be predicted within -3.66 percent at Maulap River, within 5.37 percent at Almagosa River, and within 10.74 percent at Imong River. Month-end reservoir volumes simulated by the reservoir water-balance model for both calibration and verification periods compared closely with measured reservoir volumes. Errors for the calibration periods ranged from 4.51 percent [208.7 acre-feet (acre-ft) or 68.0 million gallons (Mgal)] to -5.90 percent (-317.8 acre-ft or -103.6 Mgal). For the verification periods, errors ranged from 1.69 percent (103.5 acre-ft or 33.7 Mgal) to -4.60 percent (-178.7 acre-ft or -58.2 Mgal). Monthly simulation bias ranged from -0.19 percent for the calibration period to -0.98 percent for the verification period; relative error ranged from -0.37 to -1.12 percent, respectively. Relatively small bias indicated that the model did not consistently overestimate or underestimate reservoir volume.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20045287","collaboration":"Prepared in cooperation with the U.S. Department of the Navy","usgsCitation":"Yeung, C.W., 2005, Rainfall-Runoff and Water-Balance Models for Management of the Fena Valley Reservoir, Guam: U.S. Geological Survey Scientific Investigations Report 2004-5287, viii, 53 p., https://doi.org/10.3133/sir20045287.","productDescription":"viii, 53 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":192890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6687,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5287/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649609","contributors":{"authors":[{"text":"Yeung, Chiu W. cwyeung@usgs.gov","contributorId":2967,"corporation":false,"usgs":true,"family":"Yeung","given":"Chiu","email":"cwyeung@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":283528,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71031,"text":"fs20053090 - 2005 - Metal stocks in use in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"fs20053090","displayToPublicDate":"2005-08-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3090","title":"Metal stocks in use in the United States","language":"ENGLISH","doi":"10.3133/fs20053090","usgsCitation":"Sullivan, D.E., 2005, Metal stocks in use in the United States (Online only, Version 1.0): U.S. Geological Survey Fact Sheet 2005-3090, 2 p., https://doi.org/10.3133/fs20053090.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":121041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3090.jpg"},{"id":6683,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3090/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6272b3","contributors":{"authors":[{"text":"Sullivan, Daniel E.","contributorId":62198,"corporation":false,"usgs":true,"family":"Sullivan","given":"Daniel","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":283523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71030,"text":"sir20055069 - 2005 - Interpretation of geophysical logs, aquifer tests, and water levels in wells in and near the North Penn Area 7 Superfund site, Upper Gwynedd Township, Montgomery County, Pennsylvania, 2000-02","interactions":[],"lastModifiedDate":"2017-07-10T10:42:06","indexId":"sir20055069","displayToPublicDate":"2005-08-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5069","title":"Interpretation of geophysical logs, aquifer tests, and water levels in wells in and near the North Penn Area 7 Superfund site, Upper Gwynedd Township, Montgomery County, Pennsylvania, 2000-02","docAbstract":"Ground water in the vicinity of various industrial facilities in Upper Gwynedd Township and Lansdale Borough, Montgomery County, Pa., is contaminated with various volatile organic compounds (VOCs). The 2-square-mile area was placed on the National Priorities List as the North Penn Area 7 Superfund site by the U.S. Environmental Protection Agency (USEPA) in 1989. The U.S. Geological Survey (USGS) conducted geophysical logging, aquifer testing, water-level monitoring, and streamflow measurements in the vicinity of North Penn Area 7 beginning autumn 2000 to assist the USEPA in developing an understanding of the hydrogeologic framework in the area as part of the USEPA Remedial Investigation.\r\n\r\nThe study area is underlain by Triassic and Jurassic-age sandstones, siltstones, and shales of the Lockatong Formation and the Brunswick Group. Regionally, these rocks strike northeast and dip to the northwest. The sequence of rocks form a fractured-sedimentary-rock aquifer that acts as a set of confined to partially confined layered aquifers of differing permeabilities. The aquifers are recharged by precipitation and discharge to streams and wells. The Wissahickon Creek headwaters are less than 1 mile northeast of the study area, and this stream flows southwest to bisect North Penn Area 7. Ground water is pumped in the vicinity of North Penn Area 7 for industrial use and public supply.\r\n\r\nThe USGS collected geophysical logs for 16 wells that ranged in depth from 50 to 623 feet. Aquifer-interval-isolation testing was done in 9 of the 16 wells, for a total of 30 zones tested. A multiple-well aquifer test was conducted by monitoring the response of 14 wells to pumping a 600-ft deep production well in February and March 2002. In addition, water levels were monitored continuously in three wells in the area and streamflow was measured quarterly at two sites on Wissahickon Creek from December 2000 through September 2002. \r\n\r\nGeophysical logging identified water-bearing zones associated with high-angle fractures and bedding-plane openings throughout the depth of the boreholes. Heatpulse-flowmeter measurements under nonpumping, ambient conditions indicated that borehole flow, where detected, was in the upward direction in three of the eight wells and in the downward direction in three wells. In two wells, both upward and downward flow were measured. Heatpulse-flowmeter measurements under pumping conditions were used to identify the most productive intervals in wells. Correlation of natural-gamma-ray and single-point-resistance logs indicated that bedding in the area probably strikes about 40 degrees northeast and dips from 6 to 7 degrees northwest.\r\n\r\nAquifer intervals isolated by inflatable packers in wells were pumped to test productivity and to collect samples to determine chemical quality of water produced from the interval. Interval-isolation testing confirmed the presence of vertical hydraulic gradients indicated by heatpulse-flowmeter measurements. The specific capacities of isolated intervals ranged over two orders of magnitude, from 0.02 to more than 3.6 gallons per minute per foot. Intervals adjacent to isolated pumped intervals showed little response to pumping the isolated zone. The presence of vertical hydraulic gradients and lack of adjacent-interval response to pumping in isolated intervals indicate a limited degree of vertical hydraulic connection between the aquifer intervals tested. Concentrations of most VOC contaminants generally were highest in well-water samples from the shallowest isolated intervals, with some exceptions. Trichloroethylene, cis-1,2-dichloroethylene, and toluene were the most frequently detected VOCs, with maximum concentrations of greater than 340, 680, and greater than 590 micrograms per liter, respectively.\r\n\r\nResults of the aquifer test with multiple observation wells showed that water levels in 4 of the 14 wells declined in response to pumping. The four wells that responded to pumping are either along str","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055069","usgsCitation":"Senior, L.A., Cinotto, P.J., Conger, R.W., Bird, P.H., and Pracht, K.A., 2005, Interpretation of geophysical logs, aquifer tests, and water levels in wells in and near the North Penn Area 7 Superfund site, Upper Gwynedd Township, Montgomery County, Pennsylvania, 2000-02 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5069, 144 p., https://doi.org/10.3133/sir20055069.","productDescription":"144 p.","onlineOnly":"Y","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":193189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6682,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5069/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -40.38333333333333,75.41666666666667 ], [ -40.38333333333333,75.5 ], [ -40.333333333333336,75.5 ], [ -40.333333333333336,75.41666666666667 ], [ -40.38333333333333,75.41666666666667 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e0351","contributors":{"authors":[{"text":"Senior, Lisa A. 0000-0003-2629-1996 lasenior@usgs.gov","orcid":"https://orcid.org/0000-0003-2629-1996","contributorId":2150,"corporation":false,"usgs":true,"family":"Senior","given":"Lisa","email":"lasenior@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cinotto, Peter J. pcinotto@usgs.gov","contributorId":451,"corporation":false,"usgs":true,"family":"Cinotto","given":"Peter","email":"pcinotto@usgs.gov","middleInitial":"J.","affiliations":[{"id":354,"text":"Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Conger, Randall W. rwconger@usgs.gov","contributorId":2086,"corporation":false,"usgs":true,"family":"Conger","given":"Randall","email":"rwconger@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283520,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bird, Philip H. 0000-0003-2088-8644 phbird@usgs.gov","orcid":"https://orcid.org/0000-0003-2088-8644","contributorId":2085,"corporation":false,"usgs":true,"family":"Bird","given":"Philip","email":"phbird@usgs.gov","middleInitial":"H.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283519,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pracht, Karl A.","contributorId":102966,"corporation":false,"usgs":true,"family":"Pracht","given":"Karl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":283522,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":71033,"text":"sir20055133 - 2005 - Seepage investigation on selected reaches of Fish Creek, Teton County, Wyoming, 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"sir20055133","displayToPublicDate":"2005-08-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5133","title":"Seepage investigation on selected reaches of Fish Creek, Teton County, Wyoming, 2004","docAbstract":"A seepage investigation was conducted on Fish Creek, a tributary to the Snake River in Teton County in western Wyoming, near Wilson. Mainstem, return flow, tributary, spring, and diversion sites were selected and measured on six reaches along Fish Creek. Flow was measured under two flow regimes, high flow in August 2004 and base flow in November 2004.\r\n\r\nDuring August 17-19, 2004, 20 sites had quantifiable discharge with median values ranging from 0.93 to 384 ft3/s for the 14 mainstem sites on Fish Creek, and from 0.35 to 12.2 ft3/s for the 5 return, spring, and tributary sites (inflows). The discharge was 2.23 ft3/s for the single diversion site (outflow). Estimated gains or losses from ground water were calculated for all reaches using the median discharge values and the estimated measurement errors. Reach 1 had a calculated gain in discharge from ground water (23.8 ?3.3 ft3/s). Reaches 2-6 had no calculated gains in flow, greater than the estimated error, that could be attributed to ground water.\r\n\r\nA second set of measurements were made under base-flow conditions during November 3-4, 2004. Twelve of the 20 sites visited in August 2004 were flowing and were measured. All of the Reach 1 sites near Teton Village were dry. Median discharge values ranged from 10.3 to 70.0 ft3/s on the nine Fish Creek mainstem sites, and from 2.32 to 3.71 ft3/s on the three return, spring, and tributary sites (inflows). Reaches 2, 3 and 6 had a gain from ground water. Reaches 4 and 5 had no calculated gains in flow, greater than the estimated error, that could be attributed to ground water.","language":"ENGLISH","doi":"10.3133/sir20055133","usgsCitation":"Wheeler, J.D., and Eddy-Miller, C., 2005, Seepage investigation on selected reaches of Fish Creek, Teton County, Wyoming, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5133, 22 p., https://doi.org/10.3133/sir20055133.","productDescription":"22 p.","costCenters":[],"links":[{"id":6685,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055133/","linkFileType":{"id":5,"text":"html"}},{"id":192845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f72de","contributors":{"authors":[{"text":"Wheeler, Jerrod D. 0000-0002-0533-8700 jwheele@usgs.gov","orcid":"https://orcid.org/0000-0002-0533-8700","contributorId":1893,"corporation":false,"usgs":true,"family":"Wheeler","given":"Jerrod","email":"jwheele@usgs.gov","middleInitial":"D.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":283526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eddy-Miller, Cheryl A.","contributorId":86755,"corporation":false,"usgs":true,"family":"Eddy-Miller","given":"Cheryl A.","affiliations":[],"preferred":false,"id":283527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71032,"text":"sir20055162 - 2005 - Streamflow statistics for the Paradise and Pocono Creek watersheds and selected streamflow-gaging stations in Monroe County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-08T12:13:55","indexId":"sir20055162","displayToPublicDate":"2005-08-18T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5162","title":"Streamflow statistics for the Paradise and Pocono Creek watersheds and selected streamflow-gaging stations in Monroe County, Pennsylvania","docAbstract":" suite of 36 observed streamflow statistics, ranging from high to low flows, were computed for 7 continuous-record and predicted for 12 partial-record streamflow-gaging stations in Monroe County, Pa. The predicted statistics for the partial-record stations were determined from regression analyses of intermittent streamflow measurements made at the partial-record stations and concurrent daily mean flows at index continuous-record stations. The prediction methodology has been previously used only for estimating low-flow statistics. Results from this study indicate the methodology may have applicability for predicting high- and intermediate-flow statistics as well. Three sets of base-flow measurements were made at 40 sites in the Paradise and Pocono Creek watersheds to determine subbasin yields and stream reaches gaining or losing flow. Subbasin yields, the base-flow measurements normalized to respective drainage areas, were consistent for each measurement period.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055162","usgsCitation":"Thompson, R., and Cavallo, G.J., 2005, Streamflow statistics for the Paradise and Pocono Creek watersheds and selected streamflow-gaging stations in Monroe County, Pennsylvania: U.S. Geological Survey Scientific Investigations Report 2005-5162, 25 p., https://doi.org/10.3133/sir20055162.","productDescription":"25 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":192816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6684,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5162/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d21","contributors":{"authors":[{"text":"Thompson, Ronald E.","contributorId":27958,"corporation":false,"usgs":true,"family":"Thompson","given":"Ronald E.","affiliations":[],"preferred":false,"id":283524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cavallo, Gregory J.","contributorId":65182,"corporation":false,"usgs":true,"family":"Cavallo","given":"Gregory","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":283525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71023,"text":"fs20043099 - 2005 - Rates of landsliding and cliff retreat along the Big Sur Coast, California— Measuring a crucial baseline","interactions":[],"lastModifiedDate":"2021-11-17T22:36:48.575548","indexId":"fs20043099","displayToPublicDate":"2005-08-17T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-3099","title":"Rates of landsliding and cliff retreat along the Big Sur Coast, California— Measuring a crucial baseline","docAbstract":"No abstract available.
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Screening levels were calculated for contaminants that do not have Maximum Contaminant Level values using a consensus approach that entailed (1) standard USEPA Office of Water methodologies (equations) for establishing Lifetime Health Advisory (LHA) and Risk-Specific Dose (RSD) values for the protection of human health, and (2) existing USEPA human-health toxicity information.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20053059","usgsCitation":"Toccalino, P., Zogorski, J.S., and Norman, J.E., 2005, Health-Based Screening Levels and their Application to Water-Quality Data: U.S. Geological Survey Fact Sheet 2005-3059, 2 p., https://doi.org/10.3133/fs20053059.","productDescription":"2 p.","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":121038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3059.jpg"},{"id":11744,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3059/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6340bd","contributors":{"authors":[{"text":"Toccalino, Patricia L. 0000-0003-1066-1702","orcid":"https://orcid.org/0000-0003-1066-1702","contributorId":41089,"corporation":false,"usgs":true,"family":"Toccalino","given":"Patricia L.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":283501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":283499,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norman, Julia E. 0000-0002-2820-6225 jnorman@usgs.gov","orcid":"https://orcid.org/0000-0002-2820-6225","contributorId":3832,"corporation":false,"usgs":true,"family":"Norman","given":"Julia","email":"jnorman@usgs.gov","middleInitial":"E.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":283500,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":71026,"text":"fs20053070 - 2005 - Assessment of undiscovered oil and gas resources of the U.S. portion of the Michigan Basin, 2004","interactions":[],"lastModifiedDate":"2018-10-29T11:36:20","indexId":"fs20053070","displayToPublicDate":"2005-08-17T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3070","title":"Assessment of undiscovered oil and gas resources of the U.S. portion of the Michigan Basin, 2004","docAbstract":"No abstract available.
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","language":"Spanish","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053009S","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Evaluacion de los Recursos Potenciales de Petroleo y Gas en la Cuenca Norte de Cuba, Cuba, 2004: U.S. Geological Survey Fact Sheet 2005-3009, 2 p., https://doi.org/10.3133/fs20053009S.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":121037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3009.jpg"},{"id":6677,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3009/508FS05-3009.html","linkFileType":{"id":5,"text":"html"}},{"id":402250,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70491.htm","linkFileType":{"id":5,"text":"html"}}],"country":"Cuba","otherGeospatial":"North Cuba Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.24267578125,\n 21.43261686447735\n ],\n [\n -79.70581054687499,\n 21.43261686447735\n ],\n [\n -79.70581054687499,\n 24.026396666017327\n ],\n [\n -86.24267578125,\n 24.026396666017327\n ],\n [\n -86.24267578125,\n 21.43261686447735\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb117","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70238571,"text":"70238571 - 2005 - Comment on “Comparison between probabilistic seismic hazard analysis and flood frequency analysis”","interactions":[],"lastModifiedDate":"2022-11-29T20:21:54.074986","indexId":"70238571","displayToPublicDate":"2005-08-16T14:17:51","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7458,"text":"Eos Science News","active":true,"publicationSubtype":{"id":10}},"title":"Comment on “Comparison between probabilistic seismic hazard analysis and flood frequency analysis”","docAbstract":"Despite providing an exceptionally clear example of the basics of probabilistic seismic hazard analysis (PSHA), Wang and Ormsbee [2005] nevertheless conclude that “…using PSHA for risk analysis is not only confusing, but is also inappropriate.” I argue here that (1) the results of a PSHA analysis are not confusing and have physical meaning, and (2) the authors' basis for declaring PSHA “inappropriate” is misguided. I note in passing that the authors consistently confuse “risk” with “hazard.” Both PSHA and flood frequency analysis provide estimates of hazard. Risk is the product of hazard, vulnerability and exposure. This discussion is only concerned with hazard.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005EO330004","usgsCitation":"Holzer, T.L., 2005, Comment on “Comparison between probabilistic seismic hazard analysis and flood frequency analysis”: Eos Science News, v. 86, no. 33, p. 303-303, https://doi.org/10.1029/2005EO330004.","productDescription":"1 p.","startPage":"303","endPage":"303","costCenters":[],"links":[{"id":477653,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005eo330004","text":"Publisher Index Page"},{"id":409812,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","issue":"33","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","contributors":{"authors":[{"text":"Holzer, Thomas L. tholzer@usgs.gov","contributorId":2829,"corporation":false,"usgs":true,"family":"Holzer","given":"Thomas","email":"tholzer@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70170839,"text":"70170839 - 2005 - Characterization of a C3a receptor in rainbow trout and Xenopus: The first identification of C3a receptors in nonmammalian species","interactions":[],"lastModifiedDate":"2020-10-16T16:27:59.30422","indexId":"70170839","displayToPublicDate":"2005-08-15T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2350,"text":"Journal of Immunology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Characterization of a C3a receptor in rainbow trout and Xenopus: The first identification of C3a receptors in nonmammalian species","title":"Characterization of a C3a receptor in rainbow trout and Xenopus: The first identification of C3a receptors in nonmammalian species","docAbstract":"Virtually nothing is known about the structure, function, and evolutionary origins of the C3aR in nonmammalian species. Because C3aR and C5aR are thought to have arisen from the same common ancestor, the recent characterization of a C5aR in teleost fish implied the presence of a C3aR in this animal group. In this study we report the cloning of a trout cDNA encoding a 364-aa molecule (TC3aR) that shows a high degree of sequence homology and a strong phylogenetic relationship with mammalian C3aRs. Northern blotting demonstrated that TC3aR was expressed primarily in blood leukocytes. Flow cytometric analysis and immunofluorescence microscopy showed that Abs raised against TC3aR stained to a high degree all blood B lymphocytes and, to a lesser extent, all granulocytes. More importantly, these Abs inhibited trout C3a-mediated intracellular calcium mobilization in trout leukocytes. A fascinating structural feature of TC3aR is the lack of a significant portion of the second extracellular loop (ECL2). In all C3aR molecules characterized to date, the ECL2 is exceptionally large when compared with the same region of C5aR. However, the exact function of the extra portion of ECL2 is unknown. The lack of this segment in TC3aR suggests that the extra piece of ECL2 was not necessary for the interaction of the ancestral C3aR with its ligand. Our findings represent the first C3aR characterized in nonmammalian species and support the hypothesis that if C3aR and C5aR diverged from a common ancestor, this event occurred before the emergence of teleost fish.
","language":"English","publisher":"The American Association of Immunologists","doi":"10.4049/jimmunol.175.4.2427","usgsCitation":"Boshra, H., Wang, T., Hove-Madsen, L., Hansen, J.D., Li, J., Matlapudi, A., Secombes, C.J., Tort, L., and Sunyer, J.O., 2005, Characterization of a C3a receptor in rainbow trout and Xenopus: The first identification of C3a receptors in nonmammalian species: Journal of Immunology, v. 175, no. 4, p. 2427-2437, https://doi.org/10.4049/jimmunol.175.4.2427.","productDescription":"11 p.","startPage":"2427","endPage":"2437","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":320935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"175","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5729cbaee4b0b13d3919a2e7","contributors":{"authors":[{"text":"Boshra, Hani","contributorId":169019,"corporation":false,"usgs":false,"family":"Boshra","given":"Hani","email":"","affiliations":[],"preferred":false,"id":628628,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wang, Tiehui","contributorId":169138,"corporation":false,"usgs":false,"family":"Wang","given":"Tiehui","email":"","affiliations":[],"preferred":false,"id":628629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hove-Madsen, Leif","contributorId":169139,"corporation":false,"usgs":false,"family":"Hove-Madsen","given":"Leif","email":"","affiliations":[],"preferred":false,"id":628630,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hansen, John D. 0000-0002-3006-2734 jhansen@usgs.gov","orcid":"https://orcid.org/0000-0002-3006-2734","contributorId":3440,"corporation":false,"usgs":true,"family":"Hansen","given":"John","email":"jhansen@usgs.gov","middleInitial":"D.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":628631,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Li, Jun","contributorId":169020,"corporation":false,"usgs":false,"family":"Li","given":"Jun","email":"","affiliations":[],"preferred":false,"id":628632,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Matlapudi, Anjun","contributorId":169140,"corporation":false,"usgs":false,"family":"Matlapudi","given":"Anjun","affiliations":[],"preferred":false,"id":628633,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Secombes, Christopher J.","contributorId":169141,"corporation":false,"usgs":false,"family":"Secombes","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":628634,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tort, Lluis","contributorId":169142,"corporation":false,"usgs":false,"family":"Tort","given":"Lluis","email":"","affiliations":[],"preferred":false,"id":628635,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sunyer, J. Oriol","contributorId":169023,"corporation":false,"usgs":false,"family":"Sunyer","given":"J.","email":"","middleInitial":"Oriol","affiliations":[],"preferred":false,"id":628636,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":71015,"text":"ofr20051228 - 2005 - Evaluation of oxygen and carbon isotopes in sediments from Bear Lake, Utah and Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"ofr20051228","displayToPublicDate":"2005-08-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1228","title":"Evaluation of oxygen and carbon isotopes in sediments from Bear Lake, Utah and Idaho","language":"ENGLISH","doi":"10.3133/ofr20051228","usgsCitation":"Bright, J., and Kaufman, D., 2005, Evaluation of oxygen and carbon isotopes in sediments from Bear Lake, Utah and Idaho (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1228, 9 p., https://doi.org/10.3133/ofr20051228.","productDescription":"9 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":192659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6674,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1228/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fac82","contributors":{"authors":[{"text":"Bright, Jordon","contributorId":76010,"corporation":false,"usgs":true,"family":"Bright","given":"Jordon","affiliations":[],"preferred":false,"id":283492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufman, Darrell","contributorId":65557,"corporation":false,"usgs":true,"family":"Kaufman","given":"Darrell","affiliations":[],"preferred":false,"id":283491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71017,"text":"ofr20051226 - 2005 - Ostracodes in core BL00-1-D from Bear Lake, Utah and Idaho: preliminary analyses","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"ofr20051226","displayToPublicDate":"2005-08-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1226","title":"Ostracodes in core BL00-1-D from Bear Lake, Utah and Idaho: preliminary analyses","language":"ENGLISH","doi":"10.3133/ofr20051226","usgsCitation":"Bright, J., and Kaufman, D., 2005, Ostracodes in core BL00-1-D from Bear Lake, Utah and Idaho: preliminary analyses (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1226, 5 p., https://doi.org/10.3133/ofr20051226.","productDescription":"5 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":193071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6676,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1226/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a548","contributors":{"authors":[{"text":"Bright, Jordon","contributorId":76010,"corporation":false,"usgs":true,"family":"Bright","given":"Jordon","affiliations":[],"preferred":false,"id":283497,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufman, Darrell","contributorId":65557,"corporation":false,"usgs":true,"family":"Kaufman","given":"Darrell","affiliations":[],"preferred":false,"id":283496,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71011,"text":"sir20055021 - 2005 - Trends in timing, magnitude, and duration of summer and fall/winter streamflows for unregulated coastal river basins in Maine during the 20th century","interactions":[],"lastModifiedDate":"2022-09-09T18:13:46.255894","indexId":"sir20055021","displayToPublicDate":"2005-08-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5021","title":"Trends in timing, magnitude, and duration of summer and fall/winter streamflows for unregulated coastal river basins in Maine during the 20th century","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with the Maine Atlantic Salmon Commission (ASC), began a study in 2003 to examine the timing, magnitude, and duration of summer (June through October) and fall/early winter (September through January) seasonal streamflows of unregulated coastal river basins in Maine and to correlate them to meteorological variables and winter/spring (January through May) seasonal streamflows. This study overlapped the summer seasonal window with the fall/early winter seasonal window to completely bracket the low-streamflow period during July, August, and September between periods of high streamflows in June and October. The ASC is concerned with the impacts of potentially changing meteorological and hydrologic conditions on Atlantic salmon survival. Because winter/spring high streamflows appear to have trended toward earlier dates over the 20th century in coastal Maine, it was hypothesized that the spring/summer recession to low streamflows could have a similar trend toward earlier, and possibly lower, longer lasting, late summer/early fall low streamflows during the 20th century. \r\n\r\nThere were few statistically significant trends in the timing, magnitude, or duration of summer low streamflows for coastal river basins in Maine during the 20th century. The hypothesis that earlier winter/spring high streamflows may result in earlier or lower low streamflows is not supported by the data. No statistically significant trends in the magnitude of total runoff volume during the low-streamflow months of August and September were observed. The magnitude and timing of summer low streamflows correlated with the timing of fall/winter high streamflows and the amount of summer precipitation. The magnitude and timing of summer low streamflows did not correlate with the timing of spring snowmelt runoff. There were few correlations between the magnitude and timing of summer low streamflows and monthly mean surface air temperatures.\r\n\r\nThere were few statistically significant trends in the timing or duration of fall/winter high streamflows for coastal river basins in Maine during the 20th century. The timing of the bulk of fall/winter high streamflows correlated with seasonal precipitation. Earlier fall/winter center-of-volume dates correlated with higher September and October precipitation. In general, little evidence was observed of trends in the magnitude of seasonal runoff volume during fall/winter. The magnitude of fall/winter high streamflows positively correlated with November and December precipitation amounts. There were few correlations between the magnitude and timing of fall/winter high streamflows and monthly mean surface air temperatures.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055021","usgsCitation":"Dudley, R.W., and Hodgkins, G.A., 2005, Trends in timing, magnitude, and duration of summer and fall/winter streamflows for unregulated coastal river basins in Maine during the 20th century: U.S. Geological Survey Scientific Investigations Report 2005-5021, v, 26 p., https://doi.org/10.3133/sir20055021.","productDescription":"v, 26 p.","costCenters":[],"links":[{"id":192578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406474,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73810.htm","linkFileType":{"id":5,"text":"html"}},{"id":6671,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5021/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.55419921875,\n 42.90816007196054\n ],\n [\n -69.4775390625,\n 43.723474896114794\n ],\n [\n -67.65380859375,\n 44.19795903948531\n ],\n [\n -66.70898437499999,\n 44.68427737181225\n ],\n [\n -67.19238281249999,\n 45.19752230305682\n ],\n [\n -67.74169921875,\n 45.69083283645816\n ],\n [\n -71.08154296875,\n 43.96119063892024\n ],\n [\n -70.72998046875,\n 42.94033923363181\n ],\n [\n -70.55419921875,\n 42.90816007196054\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0779","contributors":{"authors":[{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283484,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71014,"text":"sir20055164 - 2005 - Seepage study of McLeod Creek and East Canyon Creek near Park City, Summit County, Utah, 2004","interactions":[],"lastModifiedDate":"2019-12-30T13:55:59","indexId":"sir20055164","displayToPublicDate":"2005-08-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5164","title":"Seepage study of McLeod Creek and East Canyon Creek near Park City, Summit County, Utah, 2004","docAbstract":"Seepage investigations on McLeod Creek downstream of U.S. Geological Survey streamflow-gaging station McLeod Creek near Park City, Utah, and its confluence with Kimball Creek during the summer of 2004 indicate that this section of the creek is a gaining reach. The total seepage gains ranged from 1.8 to 2.7 cubic feet per second, or a 32 to 55 percent gain. The apparent average total seepage gain was 2.2 cubic feet per second, or an average 42 percent gain. Seepage investigations from the U.S. Geological Survey streamflow-gaging station at East Canyon Creek below I-80 Rest Stop near Park City, Utah, to the station at East Canyon Creek near Jeremy Ranch, Utah, indicate that this section of East Canyon Creek is a slightly losing reach. The total seepage losses ranged from -1.2 to -2.0 cubic feet per second. This is a loss of between -18 and -27 percent from discharge measured at the upstream gaging station. The apparent average total seepage loss for the reach was -1.0 cubic feet per second, or -18 percent. Seepage information also was obtained along East Canyon Creek by using water-temperature data recorded in three shallow streambed piezometers. Surface-water temperature also was recorded at these locations. These water-temperature profiles indicate a seepage loss at all three locations along East Canyon Creek. This seepage loss appears to decrease in September and October.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055164","collaboration":"Prepared in cooperation with the Snyderville Basin Water Reclamation District","usgsCitation":"Wilkowske, C., 2005, Seepage study of McLeod Creek and East Canyon Creek near Park City, Summit County, Utah, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5164, iv, 26 p., https://doi.org/10.3133/sir20055164.","productDescription":"iv, 26 p.","numberOfPages":"33","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":192619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6673,"rank":100,"type":{"id":15,"text":"Index 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California Water Science Center, Sacramento Laboratory - determination of haloacetic acid formation potential, method validation, and quality-control practices","docAbstract":"An analytical method for the determination of haloacetic acid formation potential of water samples has been developed by the U.S. Geological Survey California Water Science Center Sacramento Laboratory. The haloacetic acid formation potential is measured by dosing water samples with chlorine under specified conditions of pH, temperature, incubation time, darkness, and residual-free chlorine. The haloacetic acids formed are bromochloroacetic acid, bromodichloroacetic acid, dibromochloroacetic acid, dibromoacetic acid, dichloroacetic acid, monobromoacetic acid, monochloroacetic acid, tribromoacetic acid, and trichloroacetic acid. They are extracted, methylated, and then analyzed using a gas chromatograph equipped with an electron capture detector. Method validation experiments were performed to determine the method accuracy, precision, and detection limit for each of the compounds. Method detection limits for these nine haloacetic acids ranged from 0.11 to 0.45 microgram per liter. Quality-control practices include the use of blanks, quality-control samples, calibration verification standards, surrogate recovery, internal standard, matrix spikes, and duplicates.","language":"ENGLISH","doi":"10.3133/sir20055115","usgsCitation":"Zazzi, B.C., Crepeau, K.L., Fram, M.S., and Bergamaschi, B., 2005, Method of analysis at the U.S. Geological Survey California Water Science Center, Sacramento Laboratory - determination of haloacetic acid formation potential, method validation, and quality-control practices (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5115, 28 p., https://doi.org/10.3133/sir20055115.","productDescription":"28 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6672,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5115/","linkFileType":{"id":5,"text":"html"}},{"id":192618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629f2c","contributors":{"authors":[{"text":"Zazzi, Barbara C.","contributorId":73689,"corporation":false,"usgs":true,"family":"Zazzi","given":"Barbara","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":283489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crepeau, Kathryn L. kcrepeau@usgs.gov","contributorId":3943,"corporation":false,"usgs":true,"family":"Crepeau","given":"Kathryn","email":"kcrepeau@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":283487,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fram, Miranda S. 0000-0002-6337-059X mfram@usgs.gov","orcid":"https://orcid.org/0000-0002-6337-059X","contributorId":1156,"corporation":false,"usgs":true,"family":"Fram","given":"Miranda","email":"mfram@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283486,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bergamaschi, Brian A. 0000-0002-9610-5581","orcid":"https://orcid.org/0000-0002-9610-5581","contributorId":73241,"corporation":false,"usgs":true,"family":"Bergamaschi","given":"Brian A.","affiliations":[],"preferred":false,"id":283488,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":71016,"text":"ofr20051227 - 2005 - Ostracode analysis for cores BL96-1 and BL96-2 from Bear Lake, Utah and Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"ofr20051227","displayToPublicDate":"2005-08-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1227","title":"Ostracode analysis for cores BL96-1 and BL96-2 from Bear Lake, Utah and Idaho","language":"ENGLISH","doi":"10.3133/ofr20051227","usgsCitation":"Bright, J., Forester, R., and Kaufman, D., 2005, Ostracode analysis for cores BL96-1 and BL96-2 from Bear Lake, Utah and Idaho (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1227, 13 p., https://doi.org/10.3133/ofr20051227.","productDescription":"13 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":192660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6675,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1227/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4c6","contributors":{"authors":[{"text":"Bright, Jordon","contributorId":76010,"corporation":false,"usgs":true,"family":"Bright","given":"Jordon","affiliations":[],"preferred":false,"id":283495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Forester, Richard","contributorId":59523,"corporation":false,"usgs":true,"family":"Forester","given":"Richard","affiliations":[],"preferred":false,"id":283493,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaufman, Darrell","contributorId":65557,"corporation":false,"usgs":true,"family":"Kaufman","given":"Darrell","affiliations":[],"preferred":false,"id":283494,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70998,"text":"ofr20041326 - 2005 - Atrazine concentrations in stream water and streambed sediment pore water in the St. Joseph and Galien River basins, Michigan and Indiana, May 2001-September 2003","interactions":[],"lastModifiedDate":"2016-09-22T15:09:46","indexId":"ofr20041326","displayToPublicDate":"2005-08-07T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1326","title":"Atrazine concentrations in stream water and streambed sediment pore water in the St. Joseph and Galien River basins, Michigan and Indiana, May 2001-September 2003","docAbstract":"The U.S. Geological Survey (USGS) sampled multiple stream sites across the St. Joseph and Galien River Basins to detect and quantify the herbicide atrazine using a field enzyme-linked immunosorbent assay (ELISA) triazine test. In May 2001, July 2001, April 2002, August 2002, August 2003 and September 2003, composite samples were collected across streams at USGS streamflow-gaging stations. Concentrations and instantaneous loading for atrazine sampled in stream water throughout the St. Joseph River and Galien River Basins in Michigan and Indiana ranged from nondetection (< 0.05 part per billion (ppb)) with an associated load less than 0.001 kilogram per day (kg/d) to 6 ppb and a maximum load of 10 kg/d. Atrazine concentrations were highest in May 2001 just after the planting season. The lowest concentration was found in April 2002 just before planting. Atrazine concentrations in streambed-sediment pore water were not spatially connected with atrazine concentrations in stream-water samples. This study showed that atrazine concentrations were elevated from May to July in the St. Joseph and Galien River Basins. At many sites, concentrations exceeded the level that has been shown to feminize frog populations (0.2 ppb). There were 8 sites where concentrations exceeded 0.2 ppb atrazine in May 2001 and July 2001.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041326","collaboration":"Prepared in Cooperation with the Michigan Department of Environmental Quality","usgsCitation":"Duris, J.W., Reeves, H.W., and Kiesler, J.L., 2005, Atrazine concentrations in stream water and streambed sediment pore water in the St. Joseph and Galien River basins, Michigan and Indiana, May 2001-September 2003: U.S. Geological Survey Open-File Report 2004-1326, iv, 19 p., https://doi.org/10.3133/ofr20041326.","productDescription":"iv, 19 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":185669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041326.JPG"},{"id":6646,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1326/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Indiana, Michigan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.75,\n 41\n ],\n [\n -86.75,\n 42.5\n ],\n [\n -84.5,\n 42.5\n ],\n [\n -84.5,\n 41\n ],\n [\n -86.75,\n 41\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6692e5","contributors":{"authors":[{"text":"Duris, Joseph W. 0000-0002-8669-8109 jwduris@usgs.gov","orcid":"https://orcid.org/0000-0002-8669-8109","contributorId":1981,"corporation":false,"usgs":true,"family":"Duris","given":"Joseph","email":"jwduris@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":false,"id":283466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, Howard W. 0000-0001-8057-2081 hwreeves@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-2081","contributorId":2307,"corporation":false,"usgs":true,"family":"Reeves","given":"Howard","email":"hwreeves@usgs.gov","middleInitial":"W.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kiesler, James L. jkiesler@usgs.gov","contributorId":4470,"corporation":false,"usgs":true,"family":"Kiesler","given":"James","email":"jkiesler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":283468,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70999,"text":"ofr20051267 - 2005 - Extent of a mine contamination plume on the Willow Creek floodplain, Creede, Colorado, as determined by willow leaf analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"ofr20051267","displayToPublicDate":"2005-08-07T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1267","title":"Extent of a mine contamination plume on the Willow Creek floodplain, Creede, Colorado, as determined by willow leaf analysis","language":"ENGLISH","doi":"10.3133/ofr20051267","usgsCitation":"Erdman, J.A., Vradenburg, L.A., and Smith, S.C., 2005, Extent of a mine contamination plume on the Willow Creek floodplain, Creede, Colorado, as determined by willow leaf analysis (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1267, 24 p., https://doi.org/10.3133/ofr20051267.","productDescription":"24 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":185670,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6647,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1267/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8a91","contributors":{"authors":[{"text":"Erdman, James A.","contributorId":37748,"corporation":false,"usgs":true,"family":"Erdman","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":283470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vradenburg, Leigh Ann","contributorId":35813,"corporation":false,"usgs":true,"family":"Vradenburg","given":"Leigh","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":283469,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Shea Clark","contributorId":50971,"corporation":false,"usgs":true,"family":"Smith","given":"Shea","email":"","middleInitial":"Clark","affiliations":[],"preferred":false,"id":283471,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70995,"text":"sir20055124 - 2005 - Hydrogeology, water quality, and water-supply potential of the Lower Floridan Aquifer, coastal Georgia, 1999-2002","interactions":[],"lastModifiedDate":"2017-01-12T09:17:52","indexId":"sir20055124","displayToPublicDate":"2005-08-07T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5124","title":"Hydrogeology, water quality, and water-supply potential of the Lower Floridan Aquifer, coastal Georgia, 1999-2002","docAbstract":"The hydrogeology and water quality of the upper permeable and Fernandina permeable zones of the Lower Floridan aquifer were studied at seven sites in the 24-county study area encompassed by the Georgia Coastal Sound Science Initiative. Although substantially less than the Upper Floridan aquifer in coastal Georgia, transmissivities for the Lower Floridan aquifer are in the same range as other water-supply aquifers in Georgia and South Carolina and could meet the needs of public drinking-water supply. Water of the upper permeable zone of the Lower Floridan aquifer exceeds the Federal secondary drinking-water standards for sulfate and total dissolved solids at most coastal Georgia sites and the Federal secondary drinking-water standard for chloride at the Shellman Bluff site.\r\n\r\nThe top of the Lower Floridan aquifer correlates within 50 feet of the previously reported top, except at the St Simons Island site where the top is more than 80 feet higher. Based on the hydrogeologic characteristics, the seven sites are divided into the northern sites at Shellman Bluff, Richmond Hill, Pembroke, and Pineora; and southern sites at St Marys, Brunswick, and St Simons Island. At the northern sites, the Lower Floridan aquifer does not include the Fernandina permeable zone, is thinner than the overlying Upper Floridan aquifer, and consists of only strata of the middle Eocene Avon Park Formation. Transmissivities in the Lower Floridan aquifer are 8,300 feet squared per day at Richmond Hill and 6,000 feet squared per day at Shellman Bluff, generally one tenth the transmissivity of the Upper Floridan aquifer at these sites. At the southern sites, the upper permeable zone of the Lower Floridan aquifer is thicker than the Upper Floridan aquifer and consists of porous limestone and dolomite interbedded with nonporous strata of the middle Eocene Avon Park and early Eocene Oldsmar Formations. Transmissivities for the upper permeable zone of the Lower Floridan aquifer are 500 feet squared per day at the St Simons Island site and 13,000 feet squared per day at the St Marys site. The Lower Floridan aquifer at the Brunswick and St Marys sites includes the Fernandina permeable zone, which consists of saltwater-bearing dolomite.\r\n\r\nHydrographs of Coastal Sound Science Initiative wells and other nearby wells open to the Upper Floridan aquifer, and the upper permeable and Fernandina permeable zones of the Lower Floridan aquifer have similar trends. Water levels in wells open to the Upper and Lower Floridan aquifers are below land surface at the northern sites and the St Simons Island site, and above land surface at the Brunswick and St Marys sites, as of January 1, 2004.\r\n\r\nFreshwater is present in the Lower Floridan aquifer at Pineora, Pembroke, and St Marys, and from 1,259 to 1,648 feet below land surface at Brunswick. Slightly saline water is present in the Lower Floridan aquifer at Richmond Hill, Shellman Bluff, St Simons Island, and from 1,679 to 1,970 feet below land surface in well 34H495 at Brunswick. The upper permeable zone of the Lower Floridan aquifer contains bicarbonate water at the Pembroke site, sulfate-bicarbonate water at the Brunswick site, and sulfate water at the St Simons Island, Shellman Bluff, St Marys, and Richmond Hill sites. The bicarbonate, sulfate-bicarbonate, and sulfate waters are saturated relative to calcite and dolomite, and undersaturated with gypsum and anhydrite.\r\n\r\nThe Fernandina permeable zone in well 34H495 includes moderately saline water, very saline water, and brine. The Fernandina permeable zone of the Lower Floridan aquifer beneath downtown Brunswick contains chloride water that is slightly undersaturated to saturated with gypsum and anhydrite. Concentrations of total dissolved solids, sulfate, and chloride exceeded the Federal secondary drinking-water standards. The chloride-contaminated plumes beneath downtown Brunswick would require at least a 12- to 20-percent contribution of very saline water from the Fernandi","language":"ENGLISH","doi":"10.3133/sir20055124","usgsCitation":"Falls, W.F., Harrelson, L.G., Conlon, K.J., and Petkewich, M.D., 2005, Hydrogeology, water quality, and water-supply potential of the Lower Floridan Aquifer, coastal Georgia, 1999-2002 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5124, 98 p.; 1 plate, https://doi.org/10.3133/sir20055124.","productDescription":"98 p.; 1 plate","onlineOnly":"Y","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":6645,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5124/","linkFileType":{"id":5,"text":"html"}},{"id":185668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"Lower Floridan Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.056640625,\n 29.67850809103362\n ],\n [\n -83.056640625,\n 33.678639851675555\n ],\n [\n -80.101318359375,\n 33.678639851675555\n ],\n [\n -80.101318359375,\n 29.67850809103362\n ],\n [\n -83.056640625,\n 29.67850809103362\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6147ed","contributors":{"authors":[{"text":"Falls, W. Fred 0000-0003-2928-9795 wffalls@usgs.gov","orcid":"https://orcid.org/0000-0003-2928-9795","contributorId":107754,"corporation":false,"usgs":true,"family":"Falls","given":"W.","email":"wffalls@usgs.gov","middleInitial":"Fred","affiliations":[],"preferred":false,"id":283465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrelson, Larry G.","contributorId":70059,"corporation":false,"usgs":true,"family":"Harrelson","given":"Larry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":283464,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Conlon, Kevin J. 0000-0003-0798-368X kjconlon@usgs.gov","orcid":"https://orcid.org/0000-0003-0798-368X","contributorId":2561,"corporation":false,"usgs":true,"family":"Conlon","given":"Kevin","email":"kjconlon@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":283463,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Petkewich, Matthew D. 0000-0002-5749-6356 mdpetkew@usgs.gov","orcid":"https://orcid.org/0000-0002-5749-6356","contributorId":982,"corporation":false,"usgs":true,"family":"Petkewich","given":"Matthew","email":"mdpetkew@usgs.gov","middleInitial":"D.","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283462,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70259484,"text":"70259484 - 2005 - Recent drought tendencies in Ethiopia and equatorial-subtropical eastern Africa","interactions":[],"lastModifiedDate":"2024-10-09T16:58:46.359151","indexId":"70259484","displayToPublicDate":"2005-08-05T11:05:08","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Recent drought tendencies in Ethiopia and equatorial-subtropical eastern Africa","docAbstract":"This report presents an analysis of Ethiopian rainfall from 1960 through 2004, based on 186 gauges in Ethiopia and 373 gauges from surrounding countriesi. Substantial post1997 declines in March-September rainfall have been observed in the northeast, southeast and southwestern portions of the country, a result corroborated by several independent data sourcesii. The observed rainfall reductions have been accompanied by an increase in millions needing food aid (Figure 1). The greatest percent decrease has occurred during the Belg (March-May) season, though Kiremt (June-September) rains have also diminished in many areas. This recent dryness may be linked to a warming tendency in the southern Indian Oceaniii, and is likely to impact densely populated and/or water-insecure regions of southern and eastern Ethiopia. These areas face declines in rainfall and increasing demands on land, water and agriculture. Recent dryness, dropping coffee prices, rising population and land degradation combine to create mounting destitution that must be countered with innovative planning and policiesiv. This report is organized as follows. Section 1 provides context for our results by summarizing recent trends in food aid, precipitation and the regional climate. Section 2 quantifies the water availability situation by analyzing potentially available runoff. Section 3 describes the results of our historical rainfall analysis. Section 4 relates the observed rainfall variations to circulation and sea surface temperature patterns in the Indian and Pacific Oceans. Section 5 briefly summarizes our results.
","language":"English","publisher":"USAID","usgsCitation":"Funk, C., Senay, G., Asfaw, A., Verdin, J., Rowland, J., Korecha, D., Eilerts, G., Michaelsen, J., Amer, S., and Choularton, R., 2005, Recent drought tendencies in Ethiopia and equatorial-subtropical eastern Africa, 12 p.","productDescription":"12 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":462750,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pdf.usaid.gov/pdf_docs/PNADH997.pdf","linkFileType":{"id":5,"text":"html"}},{"id":462751,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Ethiopia","otherGeospatial":"Equatorial-subtropical Africa","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 22.112472524042943,\n 21.654772938804683\n ],\n [\n 22.02134670189892,\n -21.604079303060374\n ],\n [\n 36.67858003845541,\n -23.025718715264382\n ],\n [\n 52.702144088498756,\n -23.352854066043264\n ],\n [\n 50.48130886237331,\n -7.185306654434008\n ],\n [\n 49.16500704170396,\n 3.6266240123125293\n ],\n [\n 52.038930178050066,\n 12.519109947654002\n ],\n [\n 43.685751135020304,\n 11.989027471650338\n ],\n [\n 36.52548609424606,\n 22.343695928883136\n ],\n [\n 22.112472524042943,\n 21.654772938804683\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Funk, Chris 0000-0002-9254-6718 cfunk@usgs.gov","orcid":"https://orcid.org/0000-0002-9254-6718","contributorId":167070,"corporation":false,"usgs":true,"family":"Funk","given":"Chris","email":"cfunk@usgs.gov","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":915457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senay, Gabriel B. 0000-0002-8810-8539 senay@usgs.gov","orcid":"https://orcid.org/0000-0002-8810-8539","contributorId":166812,"corporation":false,"usgs":true,"family":"Senay","given":"Gabriel","email":"senay@usgs.gov","middleInitial":"B.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":915458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Asfaw, Alemu","contributorId":344302,"corporation":false,"usgs":false,"family":"Asfaw","given":"Alemu","email":"","affiliations":[],"preferred":false,"id":915459,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Verdin, James 0000-0003-0238-9657 verdin@usgs.gov","orcid":"https://orcid.org/0000-0003-0238-9657","contributorId":145830,"corporation":false,"usgs":true,"family":"Verdin","given":"James","email":"verdin@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":915460,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rowland, Jim 0000-0003-4837-3511","orcid":"https://orcid.org/0000-0003-4837-3511","contributorId":22891,"corporation":false,"usgs":true,"family":"Rowland","given":"Jim","email":"","affiliations":[],"preferred":false,"id":915461,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Korecha, Diriba","contributorId":195983,"corporation":false,"usgs":false,"family":"Korecha","given":"Diriba","email":"","affiliations":[],"preferred":false,"id":915462,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Eilerts, Gary","contributorId":31101,"corporation":false,"usgs":true,"family":"Eilerts","given":"Gary","email":"","affiliations":[],"preferred":false,"id":915463,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Michaelsen, Joel","contributorId":149202,"corporation":false,"usgs":false,"family":"Michaelsen","given":"Joel","affiliations":[],"preferred":false,"id":915464,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Amer, Saud A. samer@usgs.gov","contributorId":3300,"corporation":false,"usgs":true,"family":"Amer","given":"Saud A.","email":"samer@usgs.gov","affiliations":[{"id":349,"text":"International Water Resources Branch","active":true,"usgs":true}],"preferred":true,"id":915465,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Choularton, Richard","contributorId":345060,"corporation":false,"usgs":false,"family":"Choularton","given":"Richard","email":"","affiliations":[],"preferred":false,"id":915466,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ]}